Hydrogeologists evaluated the hydraulic conductivity (, in ) of four sediment types under three compaction levels (, , and ). The results are presented in the following table:
| Sediment Type | at (m/day) | at (m/day) | at (m/day) |
|---|---|---|---|
| Clay | |||
| Silt | |||
| Fine Sand | |||
| Coarse Gravel |
Statement: If this data were translated into a line graph with compaction density on the horizontal axis and hydraulic conductivity () on the vertical axis, the lines for all four sediment types would show a positive slope from left to right.
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The statement is False because higher compaction density leads to lower hydraulic conductivity for all four sediment types, which translates to a negative slope on a line graph.
The statement is incorrect because the tabular data shows an inverse relationship between compaction density and hydraulic conductivity (). As compaction density increases from left to right along the table headers (), the corresponding values decrease for all four sediment types. When translated into a line graph with density on the x-axis and on the y-axis, lines that fall from left to right exhibit a negative slope, not a positive slope.
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Translating Tabular Relationships to Graphical Slopes
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